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Paragenesis, alteration and geothermometry of the cassiterite veins of Coal Creek, Alaska
Date
1992Type
ThesisDepartment
Geological Sciences and Engineering
Degree Level
Master's Degree
Degree Name
Geology
Abstract
Hreisen bordered, quartz-cassiterite veins have formed within 52 m.y. old multiple-phase granitic intrusives. Four intrusives have been identified. The intrusives are hosted by hornfelsed argillites of the West Fork miniterrane.
Description
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Permanent link
http://hdl.handle.net/11714/1605Subject
Greisenquartz-cassiterite
veins
granitic inrusives
hornfelsed argillites
West Fork miniterrane
mineralized zones
fractures
silicification
sericite
chlorite
topaz
wolframite
quartz
cassiterite
tourmaline
arsenopyrite
pyrrhotite
sphalerite
chalcopyrite
stannite
fluorite
bismuth
galena
and proustite
deposition
Alaska
Coal Creek
Mackay Science Project
Additional Information
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